共 17 条
[1]
The transversely isotropic poroelastic wave equation including the Biot and the squirt mechanisms:Theory and application. Parra J O. Geophysics . 1997
[2]
Squirt flow in fully saturated rocks. Dvorkin J,Mavko G and Nur A. Geophysics . 1995
[3]
Attenuation by squirt flow in undersaturated gas sands. Palmer I D and Traviolia M L. Geophysics . 1980
[4]
The squirt-flow mechanism: Macroscopic description. Dvorkin J,Hoeksema N R and Nur A. Geophysics . 1994
[5]
Relating p-wave attenuation to permeability. Akbar N,Dvorkin J and Nur A. Geophysics . 1993
[6]
Theory of propagation of elastic waves in a fluid-saturated porous solid, Ⅱ Higher-frequencyrange. Biot M A. The Journal of The Acoustical Society of America . 1956
[7]
Acoustic relaxation in sedimentary rocks: Dependenceon grain contacts and fluid saturation. Murphy W F,Winkler K W and Kleinberg R L. Geophysics . 1986
[8]
The effect of viscosity of a fluid phase on velocity in low porosity rocks. Nur A and Simmons G. Earth and Planetary Science Letters . 1969
[9]
EstimationofVelocityDispersionBetweenSeismicAndUltrasonicFrequencies. WinklerKW. Geophysics . 1986
[10]
Melt squirt in asthenosphere. Mavko G and Nur A. Journal of Geophysical Research . 1975